Physical Features: Luzhou lies at the transition area between southern Sichuan Basin and Yunnan-Guizhou Plateau.
地理特征：泸州位于四川南部盆地和云贵高原的过渡区域。
Physical Features: Luzhou lies at the transition area between the southern Sichuan Basin and Yunnan-Guizhou Plateau.
地理特征：泸州位于四川南部盆地和云贵高原的过渡区域。
The overthrust belt on western border of Orduosi basin is a transition zone between North China platform and Qilian geosyncline and is special both in tec - tonic and.
鄂尔多斯盆地西缘逆冲带是介于华北陆台与祁连地槽两大构造系的过渡区。
The researches on the basin range transition thus become the frontiers of continental geology.
因此，盆山转换研究、探索盆转山和山控盆的过程则成为大陆地质的前沿研究领域。
The overthrust belt on western border of Orduosi basin is a transition zone between North China platform and Qilian geosyncline and is special both in tec- tonic and. sedimentary conditions.
鄂尔多斯盆地西缘逆冲带是介于华北陆台与祁连地槽两大构造系的过渡区。
The studies indicate that the fluid formed during the basin mountain transition is metamorphic fluid with multi phase salt water formed in the initial stage of deformation.
盆山转换时期所形成的变质流体为多相盐水流体，形成于变形的初期。
This provides strong geochemical evidences for correctly understanding the evolution of the old Tethys and the basin range transition.
从而为正确认识古特提斯洋的演化和盆山转换过程提供了强有力的地球化学证据。
This paper studies the key technologies of high-precision seismic exploration in land-water transition zone in the Liaohe Basin.
论文主要研究在辽河油田陆上水陆过渡带进行高精度地震勘探的关键技术。
The results show that 1972 is the transition point of hydrological series of Wudinghe, and human activities have affected significantly on hydrology of Wudinghe basin since 1972.
结果表明：1972年是无定河流域水文序列的突变点，1972年以后人类活动对该流域水文的影响更为显著。
Block 1 in the middle of Junggar basin show good formation conditions, developmental reservoir and complex oil-gas-water transition interface.
准噶尔盆地中部1区成藏条件较好、储层较发育、油气水过渡界面复杂。
The main layer is Putaohua Formation, deposited in the transition zone from a large delta front to lake in northern Songliao Basin.
主要含油层位是葡萄花油层，沉积时期处于松辽盆地北部大型三角洲沉积体系的前缘相带到湖相的过渡带上。
The main layer is Putaohua Formation, deposited in the transition zone from a large delta front to lake in northern Songliao Basin.
主要含油层位是葡萄花油层，沉积时期处于松辽盆地北部大型三角洲沉积体系的前缘相带到湖相的过渡带上。
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